A STRUCTURAL-GEODYNAMIC FACTOR IN THE DISTRIBUTION OF GOLD MINERALIZATION IN SOUTHERN PRIMORYE

dc.contributor.author	Utkin V.P.
dc.contributor.author	Mitrokhin A.N.
dc.contributor.author	Nevolin P.L.
dc.contributor.author	Sayadyan G.R.
dc.contributor.author	Sorokin B.K.
dc.date.accessioned	2022-07-25T04:36:27Z
dc.date.available	2022-07-25T04:36:27Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13462593
dc.identifier.citation	Doklady Earth Sciences, 2004, 395, 2, 153-156
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38401
dc.description.abstract	The constructed geologic-structural map is presented, in which one of main structures are open north-north-western fractures grouped in shear zones. The shear zones (which were especially studied) are characterized by the complex of structural and geodynamic factors (plutonic steeply dipping earth crust fractures possessing the dynamic effect of accelerated mineral-formation and substance remobilization, enhanced permeability for ore-bearing fluids and local ore-concentrating structures), which determined their dominating role in distribution of gold mineralization within Southern Primor'e.
dc.title	A STRUCTURAL-GEODYNAMIC FACTOR IN THE DISTRIBUTION OF GOLD MINERALIZATION IN SOUTHERN PRIMORYE
dc.type	Статья

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